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    Parameterization of the Vertical Transport of Momentum by Cumulus Clouds. Part I: Theory

    Source: Journal of the Atmospheric Sciences:;1991:;Volume( 048 ):;issue: 012::page 1483
    Author:
    Zhang, Guang Jun
    ,
    Cho, Han-Ru
    DOI: 10.1175/1520-0469(1991)048<1483:POTVTO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A scheme is developed to parameterize the vertical transport of momentum by cumulus clouds, in which the effect of a cloud-induced pressure field is included. In addition, a new form for momentum exchange between clouds and their environment is used. The scheme incorporates a simple cloud model which includes both updraft and downdraft and specifies the cloud dynamic fields to enable us to determine the mean pressure gradient force across the clouds. It is shown that in a typical environment with vertical wind shear, the pressure gradient force is along the direction of the wind shear. The equation governing cloud mean momentum together with the diagnostic equation for cloud-induced pressure field is solved by iteration to evaluate quantitatively the horizontal pressure gradient force across the cloud and determine the cloud mean momentum. Application of the parameterization scheme to GATE convective events will be presented in Part II of this paper.
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      Parameterization of the Vertical Transport of Momentum by Cumulus Clouds. Part I: Theory

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    contributor authorZhang, Guang Jun
    contributor authorCho, Han-Ru
    date accessioned2017-06-09T14:30:25Z
    date available2017-06-09T14:30:25Z
    date copyright1991/06/01
    date issued1991
    identifier issn0022-4928
    identifier otherams-20552.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4156793
    description abstractA scheme is developed to parameterize the vertical transport of momentum by cumulus clouds, in which the effect of a cloud-induced pressure field is included. In addition, a new form for momentum exchange between clouds and their environment is used. The scheme incorporates a simple cloud model which includes both updraft and downdraft and specifies the cloud dynamic fields to enable us to determine the mean pressure gradient force across the clouds. It is shown that in a typical environment with vertical wind shear, the pressure gradient force is along the direction of the wind shear. The equation governing cloud mean momentum together with the diagnostic equation for cloud-induced pressure field is solved by iteration to evaluate quantitatively the horizontal pressure gradient force across the cloud and determine the cloud mean momentum. Application of the parameterization scheme to GATE convective events will be presented in Part II of this paper.
    publisherAmerican Meteorological Society
    titleParameterization of the Vertical Transport of Momentum by Cumulus Clouds. Part I: Theory
    typeJournal Paper
    journal volume48
    journal issue12
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1991)048<1483:POTVTO>2.0.CO;2
    journal fristpage1483
    journal lastpage1492
    treeJournal of the Atmospheric Sciences:;1991:;Volume( 048 ):;issue: 012
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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